THE TRANSFORMATION OF QUALITATIVE COMPOSITION OF DRINKING GROUNDWATER IN THE CENTRAL PART OF DDAB

Udalov I., L. S.
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引用次数: 3

Abstract

A modern conceptual approach to a study of the ecological and hydrogeological transformation of the qualitative composition of drinking groundwater of the buchak-kaniv aquifer in the central part of Dnipro-Donetsk artesian basin in the current natural-technogenic conditions has been proposed in the article. A rational unification of the indicators that characterize geological, ecological-hydrogeological and neotectonic conditions of the territory has been done. According to these conditions – natural and technogenic factors of the water quality deterioration of the target aquifer have been identified and investigated at the present stage. The spatio-temporal patterns of changes in the chemical composition of the studied waters during the period of active complex technogenic influence on the geological environment of the region (1960-2015) have been revealed. The main pollu-tant elements of these waters have been established, with their distribution at depth and surface by genesis. The elements-indicators of qualitative composition transformation of the groundwater have been determined. The authors have traced the dynamics exhibiting an increase in its content during long-term exploitation at about 20 powerful urban water intakes within the work area. According to this approach, measures for the stabiliza-tion of the waters’ chemical composition at the buchak-kaniv water intakes of the research area have been developed. The authors justified a me-thodical approach to the prediction of groundwater ecological condition changes under the influence of the established ecological and hydrogeological factors. The measures of eco-friendly groundwater management at strategically important water intakes within the region have been proposed. Recommendations have been given for both existing and prospective water intakes.
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三峡库区中部饮用地下水质的组成变化
本文提出了一种现代概念方法来研究第聂伯-顿涅茨克自流盆地中部布恰克-卡尼夫含水层在当前自然-技术条件下饮用地下水质的生态和水文地质变化。合理统一了本区地质、生态水文地质和新构造条件的指标。根据这些条件,本阶段对目标含水层水质恶化的自然因素和技术因素进行了识别和研究。揭示了区域地质环境复杂技术影响活跃时期(1960—2015年)研究水域化学成分变化的时空格局。确定了这些水体的主要污染元素,并根据成因确定了它们在深层和表层的分布。确定了地下水定性成分转化的元素指标。作者追踪了在工作区域内大约20个强大的城市取水口长期开采期间其含量增加的动态。根据这一方法,制定了稳定研究区布加勒斯特-卡尼夫取水口水化学成分的措施。论证了在已确定的生态水文地质因素影响下预测地下水生态状况变化的方法。提出了区域内具有战略意义的重要水源地的生态地下水管理措施。对现有和未来的饮水量提出了建议。
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